Floresta Formation
| Floresta Formation | |
|---|---|
| Stratigraphic range: Late Emsian-Early Givetian ~ | |
 Platyceras nodosum from the Floresta Formation | |
| Type | Geological formation |
| Underlies | Cuche Formation |
| Overlies | El Tíbet Formation |
| Thickness | up to 600 m (2,000 ft) |
| Lithology | |
| Primary | Siltstone |
| Other | Shale, coquina, sandstone |
| Location | |
| Coordinates | 5°51′37.2″N 72°56′57.6″W / 5.860333°N 72.949333°W |
| Region | Altiplano Cundiboyacense Eastern Ranges, Andes |
| Country | Colombia |
| Type section | |
| Named for | Floresta |
| Named by | Olsson & Carter |
| Location | Floresta |
| Year defined | 1939 |
| Coordinates | 5°51′37.2″N 72°56′57.6″W / 5.860333°N 72.949333°W |
| Approximate paleocoordinates | 51°42′S 48°06′W / 51.7°S 48.1°W |
| Region | Boyacá |
| Country | Colombia |
| Thickness at type section | 600 m (2,000 ft) |
 Paleogeography of the Middle Devonian 380 Ma, by Stampfli & Borel | |
The Floresta Formation (Spanish: Formación Floresta, Df) is a geological formation of the Altiplano Cundiboyacense in the Eastern Ranges of the Colombian Andes. The sequence of siltstones, shales, coquinas and sandstone beds dates to the Devonian period; Late Emsian, Eifelian and Early Givetian epochs, and has a maximum thickness of 600 metres (2,000 ft). The unit is highly fossiliferous; brachiopods, bryozoans, gastropods, trilobites, corals and bivalves have been found in the Floresta Formation. Some fragments of Placoderm fish fossils were found in the Floresta Formation, while the overlying Cuche Formation is much richer in fish biodiversity.
Etymology
The formation was first described as Floresta Series by Olsson and Carter in 1939. The current definition was given by Botero in 1950. The formation is named after Floresta, Boyacá, where the formation outcrops.
Description
Lithologies
The Floresta Formation is characterized by a lower sequence of shales and ochre to beige siltstones with alternating coquinas, while the upper part consists of siltstones with sandy beds.
Stratigraphy and depositional environment
The Floresta Formation overlies the El Tíbet Formation and is overlain by the Cuche Formation. The age has been estimated to be Late Emsian to Early Givetian. Stratigraphically, the formation is time equivalent with the Portachuelo Formation around Quetame. The Onondaga Formation of New York is considered time equivalent too. The formation contains concretions and a high diversity of fossils. The formation was deposited in a transgressional and regressional epicontinental marine environment at the edge of the Paleo-Tethys Ocean. The uppermost part of the formation has been deposited in a deltaic setting, with the lower sequence formed in a coral reef environment.
Fossil content
Remains of Barroisella sp., ?Tarutiglossa sp., Dipleura cf. dekayi, Dechenella boteroi, Mannopyge sp., Cordania gasepiou, Viaphacops cristata, Anchiopsis armata, Synphoria stemmata, Coronura cf. lessepsensis, Greenops cf. grabaui, Belenopyge contusa, Kettneraspis callicera, Placoderm fishes, Platyceras nodosum, Acrospirifer olssoni, Anoplotheca cf. silvetii, Atrypa harrisi, Australospirifer cf. antarcticus, Aviculopecten wellsi, Brachyspirifer palmerae, Camarotoechia dotis, Chonetes cf. billingsi, C. comstockii, C. cf. stubeli, Chonostrophia knodi, Cyclotrypa boyaca, C. carribeana, C. dickeyi, C. reticulata, C. stellata, Cymostrophia dickeyi, C. schucherti, C. waringi, Cypricardinia cf. subindenta, Cyrtina hamiltonensis, Dalmanites cf. patacamayaensis, Dictyostrophia cooperi, Elytha colombiana, Eodevonaria imperialis, Favosites aff. hamiltonensis, Fenestrellina colombiana, F. olssoni, F. acuta, F. quadrata, F. harrisi, Fistulipora anomala, F. megalopora, Florestacanthus morenoi, Heliophyllum halli, Intrapora fragilis, I. megalopora, Leiorhynchus mysia, Leptaena boyaca, Meganteris australis, Megastrophia hopkinsi, M. pygmaea, Meristella wheeleri, Nucleospira concinna, Odontopleura callicera, Pentagonia gemmisulcata, Phacops cf. salteri, Pholidops florestae, Platyostoma lineata, Pleurodictyum americanum, Polypora elegantula, P. granulifera, Prismopora inornata, Schellwienella goldringae, Semicoscinium colombiensis, S. minutum, Spinocyrtia cf. valenteana, Spinulicosta spinulicosta, Spirifer kingi, Strophonella floweri, S. meridionalis, Sulcoretepora olssoni, S. subramosa, Taeniopora florestae, Tropidoleptus carinatus, Unitrypa casteri, Acanthograptus sp., Actinopteria sp, Amphigenia sp., Anthozoa indet, Camarotoechia sp., Cryptonella sp., Cyphaspis sp., Cryphaeus sp., Dalmanites sp., Derbyina sp., Gastropoda indet, Grammysia sp., Homalonotus sp., Leptostrophia sp., Mediospirifer sp., Orthoceras sp., Ostracoda indet., Orthis sp., Paraspirifer sp., Proetus sp., Pterinea sp., Strophodonta sp., Thamnopora sp., and Vitulina sp. have been described from the Floresta Formation. Colombianaspis carvalhoae gen. et sp. nov., Schizobolus pilasiensis sp. nov. and Tarijactinoides sp. nov., were newly described in 2015.
Outcrops
The Floresta Formation is found at the Floresta Massif around its type locality in Floresta, Boyacá, stretching to the south until between Busbanzá and Nobsa and to the west close to Belén, Cerinza and Tutazá. The formation is also found in the upper course of the Chicamocha River in the eponymous canyon.
Many of the fossils are on display in the paleontological museum of Floresta.
Regional correlations
- Legend
- group
- important formation
- fossiliferous formation
- minor formation
- (age in Ma)
- proximal Llanos (Medina)
- distal Llanos (Saltarin 1A well)
See also
Notes
References
- ↑ Mojica & Villarroel, 1984, p.64
- ↑ Morzadec et al., 2015, p.332
- 1 2 Morzadec et al., 2015, p.355
- ↑ Morzadec et al., 2015, p.331
- ↑ Giroud López, 2014, p.168
- ↑ Janvier & Villarroel, 1998, p.6
- ↑ Giroud López, 2014, p.169
- ↑ Giroud López, 2014, p.170
- ↑ Morzadec et al., 2015, p.335
- ↑ Morzadec et al., 2015, p.336
- ↑ Morzadec et al., 2015, p.340
- ↑ Morzadec et al., 2015, p.342
- ↑ Morzadec et al., 2015, p.344
- ↑ Morzadec et al., 2015, p.346
- ↑ Morzadec et al., 2015, p.348
- 1 2 Morzadec et al., 2015, p.352
- ↑ Janvier & Villarroel, 1998, p.9
- 1 2 Giroud López, 2014, p.39
- ↑ Floresta at Fossilworks.org
- ↑ Mojica & Villarroel, 1984, p.70
- ↑ Plancha 172, 1998
- 1 2 3 4 5 6 García González et al., 2009, p.27
- 1 2 3 4 5 6 García González et al., 2009, p.50
- 1 2 García González et al., 2009, p.85
- 1 2 3 4 5 6 7 8 9 10 Barrero et al., 2007, p.60
- 1 2 3 4 5 6 7 8 Barrero et al., 2007, p.58
- ↑ Plancha 111, 2001, p.29
- 1 2 Plancha 177, 2015, p.39
- 1 2 Plancha 111, 2001, p.26
- ↑ Plancha 111, 2001, p.24
- ↑ Plancha 111, 2001, p.23
- 1 2 Pulido & Gómez, 2001, p.32
- ↑ Pulido & Gómez, 2001, p.30
- 1 2 Pulido & Gómez, 2001, pp.21-26
- ↑ Pulido & Gómez, 2001, p.28
- ↑ Correa Martínez et al., 2019, p.49
- ↑ Plancha 303, 2002, p.27
- ↑ Terraza et al., 2008, p.22
- ↑ Plancha 229, 2015, pp.46-55
- ↑ Plancha 303, 2002, p.26
- ↑ Moreno Sánchez et al., 2009, p.53
- ↑ Mantilla Figueroa et al., 2015, p.43
- ↑ Manosalva Sánchez et al., 2017, p.84
- 1 2 Plancha 303, 2002, p.24
- 1 2 Mantilla Figueroa et al., 2015, p.42
- ↑ Arango Mejía et al., 2012, p.25
- ↑ Plancha 350, 2011, p.49
- ↑ Pulido & Gómez, 2001, pp.17-21
- ↑ Plancha 111, 2001, p.13
- ↑ Plancha 303, 2002, p.23
- ↑ Plancha 348, 2015, p.38
- ↑ Planchas 367-414, 2003, p.35
- ↑ Toro Toro et al., 2014, p.22
- ↑ Plancha 303, 2002, p.21
- 1 2 3 4 Bonilla et al., 2016, p.19
- ↑ Gómez Tapias et al., 2015, p.209
- 1 2 Bonilla et al., 2016, p.22
- 1 2 Duarte et al., 2019
- ↑ García González et al., 2009
- ↑ Pulido & Gómez, 2001
- ↑ García González et al., 2009, p.60
Bibliography
- Giroud López, Marie Joëlle (2014), El Mar en la Localidad Tipo del Devónico Medio, del Municipio de Floresta - Boyacá, Colombia, Universidad de La Habana, pp. 1–174, retrieved 2017-03-31
- Janvier, Philippe; Villarroel A, Carlos (1998), "Los Peces Devónicos del Macizo de Floresta (Boyacá, Colombia). Consideraciones taxonómicas, bioestratigráficas, biogeográficas y ambientales", Geología Colombiana, 23: 3–18, retrieved 2017-03-31
- Mojica, Jairo; Villarroel A, Carlos (1984), "Contribución al conocimiento de las unidades paleozoicas del área de Floresta (Cordillera Oriental Colombiana; Departamento de Boyacá) y en especial al de la Formación Cuche" (PDF), Geología Colombiana, 13: 55–80, archived from the original (PDF) on 2017-04-05, retrieved 2017-03-31
- Morzadec, Pierre; Mergl, Michal; Villarroel, Carlos; Janvier, Philippe; Racheboeuf, Patrick R. (2015), "Trilobites and inarticulate brachiopods from the Devonian Floresta Formation of Colombia: a review" (PDF), Bulletin of Geosciences, 90: 331–358, doi:10.3140/bull.geosci.1515, retrieved 2017-04-04
Maps
- Royero, José María; Zambrano, J.; Daconte, Rommel; Mendoza, H.; Vargas, Rodrigo (1999), Plancha 111 - Toledo - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Angarita, Leonidas; Carrillo, Víctor; Castro, Alfonso; Daconte, Rommel; Niño, Mario; Pulido, Orlando G.; Rodríguez, J. Antonio; Royero, José María; Salinas, Carlos Ulloa and Rodrigo Vargas, Rosalba (2009), Plancha 135 - San Gil - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Vargas, Rodrigo; Arias, Alfonso; Jaramillo, Luis; Tellez, Noel (1984), Plancha 136 - Málaga - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Pulido González, Orlando (2009), Plancha 151 - Charalá - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
- Ulloa, Carlos E.; Guerra, Álvaro; Escovar, Ricardo (1998), Plancha 172 - Paz de Río - 1:100,000, INGEOMINAS, p. 1, retrieved 2017-06-06
External links
- (in Spanish) Peces devónicos de Colombia, diversidad en los mares y ríos de hace 410-355 millones de años
